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Lo I Yin

Researcher at Goddard Space Flight Center

Publications -  39
Citations -  782

Lo I Yin is an academic researcher from Goddard Space Flight Center. The author has contributed to research in topics: X-ray photoelectron spectroscopy & Auger electron spectroscopy. The author has an hindex of 15, co-authored 39 publications receiving 767 citations.

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Apollo 15 Geochemical X-ray Fluorescence Experiment: Preliminary Report.

TL;DR: The results indicate the existence of a differential lunar highland crust, probably feldspathic, related to the plagioclase-rich materials previously found in the samples from Apollo 11, Apollo 12, Apollo 14, Apollo 15, and Luna 16.
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Widths of atomic M-shell vacancy states and quasiatomic aspects of radiationless transitions in solids

TL;DR: In this article, the free-atom Auger and Coster-Kronig energies have been calculated in a neutral-atom potential, and the results are consistently smaller, sometimes by a factor of 3, than expected from previous theory, and do not show the pronounced effect of predicted super-Coster Kronig transitions.
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Electron delocalization and the characterization of the L 3 MM Auger spectra of 3 d transition metals

TL;DR: In this paper, a hole localization parameter and an energy parameter were derived from the Auger spectra of metals with both open and filled $3d$ bands, which can be used to quantitatively evaluate the contributions of hole-hole interaction and relaxation, to the total energy difference between single and double-hole final states.
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X-Ray Photoelectron Spectroscopic Studies of Valence States Produced by Ion-Sputtering Reduction:

TL;DR: X-ray photoelectron spectroscopic measurements of various valence states of Fe and Cu in several compounds using ion-sputtering reduction are presented, and the potential usefulness of this time-dependent and in situ method is discussed as discussed by the authors.
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Apollo 16 geochemical x-ray fluorescence experiment: preliminary report.

TL;DR: The lunar surface was mapped with respect to magnesium, aluminum, and silicon as aluminum/ silicon and magnesium/ silicon intensity ratios along the projected ground tracks swept out by the orbiting Apollo 16 spacecraft to confirm the idea that the moon has a widespread differentiated crust (the highlands).